The PMIP 4 contribution to CMIP 6 – Part 1 : Overview and overarching analysis plan
暂无分享,去创建一个
Michel Crucifix | Sandy P. Harrison | Tianjun Zhou | Paul J. Valdes | Steven J. Phipps | Didier M. Roche | Johann H. Jungclaus | Masa Kageyama | Gavin A. Schmidt | Jean-Yves Peterschmitt | Patrick J. Bartlein | Natalie M. Mahowald | Lev Tarasov | Ayako Abe-Ouchi | Pascale Braconnot | Daniel J. Lunt | Alan M. Haywood | Hubertus Fischer | Qiong Zhang | N. Mahowald | G. Schmidt | P. Valdes | W. Peltier | B. Otto‐Bliesner | M. Kageyama | M. Crucifix | P. Braconnot | S. Harrison | P. Bartlein | S. Albani | A. Abe‐Ouchi | H. Fischer | S. Phipps | T. Zhou | J. Jungclaus | D. Lunt | C. Brierley | Qiong Zhang | L. Tarasov | A. Haywood | P. Bartlein | R. Ivanovic | P. Hopcroft | F. Lambert | D. Roche | W. Richard Peltier | Bette L. Otto-Bliesner | A. Dolan | Ruza F. Ivanovic | Samuel Albani | Chris Brierley | Aisling Dolan | Laura Fernandez-Donado | Peter O. Hopcroft | Fabrice Lambert | J. Peterschmitt | L. Fernández-Donado | Qiong Zhang | R. Ivanović | Fabrice Lambert | Samuel Albani | B. L. Otto-Bliesner | Paul J. Valdes | G. A. Schmidt | Masa Kageyama | Sandy P. Harrison | Chris M. Brierley | Hubertus Fischer | D. J. Lunt | W. R. Peltier | Lev Tarasov | Tianjun Zhou | Patrick J. Bartlein
[1] P. Braconnot,et al. Changes in the ENSO/SPCZ relationship from past to future climates , 2015 .
[2] P. Valdes,et al. Last glacial maximum constraints on the Earth System model HadGEM2-ES , 2015, Climate Dynamics.
[3] Fiona Tummon,et al. The Model Intercomparison Project on the climatic response to Volcanic forcing (VolMIP) : experimental design and forcing input data for CMIP6 , 2016 .
[4] A. Timmermann,et al. On the definition of seasons in paleoclimate simulations with orbital forcing , 2008 .
[5] Andrew D. Jones,et al. Lawrence Berkeley National Laboratory Recent Work Title The Land Use Model Intercomparison Project ( LUMIP ) contribution to CMIP 6 : Rationale and experimental design Permalink , 2016 .
[6] Harry J. Dowsett,et al. High eustatic sea level during the middle Pliocene:Evidence from the southeastern U.S. Atlantic Coastal Plain , 1990 .
[7] G. Wilson,et al. Constraints on the amplitude of Mid-Pliocene (3.6–2.4 Ma) eustatic sea-level fluctuations from the New Zealand shallow-marine sediment record , 2009, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[8] Sandy P. Harrison,et al. Simulation of tree-ring widths with a model for primary production, carbon allocation, and growth , 2014 .
[9] M. Chandler,et al. Mid-Pliocene sea level and continental ice volume based on coupled benthic Mg/Ca palaeotemperatures and oxygen isotopes , 2009, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[10] G. Messori,et al. Impacts of dust reduction on the northward expansion of the African monsoon during the Green Sahara period , 2016 .
[11] A. Timmermann,et al. The response of ENSO flavors to mid‐Holocene climate: Implications for proxy interpretation , 2015 .
[12] W. Collins,et al. Evaluation of climate models , 2013 .
[13] M. Huber,et al. Spontaneous transition to superrotation in warm climates simulated by CAM3 , 2010 .
[14] B. Hönisch,et al. Atmospheric CO2 decline during the Pliocene intensification of Northern Hemisphere glaciations , 2011 .
[15] M. Schulz,et al. Last interglacial temperature evolution - a model inter-comparison , 2012 .
[16] J. Kutzbach,et al. Sensitivity of a coupled atmosphere/mixed layer ocean model to changes in orbital forcing at 9000 years B.P. , 1988 .
[17] H. Renssen,et al. Evaluating Southern Ocean sea-ice for the Last Glacial Maximum and pre-industrial climates: PMIP-2 models and data evidence , 2012 .
[18] P. Friedlingstein,et al. Modeling fire and the terrestrial carbon balance , 2011 .
[19] A. Mackensen,et al. Alkenone and boron based Pliocene pCO2 records , 2010 .
[20] Margo Project Members. Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum , 2009 .
[21] Karl E. Taylor,et al. An overview of CMIP5 and the experiment design , 2012 .
[22] W. Peltier,et al. Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model , 2015 .
[23] Rainer Zahn,et al. Atlantic Meridional Overturning Circulation During the Last Glacial Maximum , 2007, Science.
[24] C. Turney,et al. Does the Agulhas Current amplify global temperatures during super‐interglacials? , 2010 .
[25] Patrick Heimbach,et al. OMIP contribution to CMIP6: experimental and diagnostic protocol for the physical component of the Ocean Model Intercomparison Project , 2016 .
[26] J. Kutzbach,et al. Calendar effect on phase study in paleoclimate transient simulation with orbital forcing , 2011 .
[27] P. deMenocal,et al. The magnitude, timing and abruptness of changes in North African dust deposition over the last 20,000 yr , 2013 .
[28] G. Ramstein,et al. Large-scale features of Pliocene climate: results from the Pliocene Model Intercomparison Project , 2012 .
[29] D. Krantz. A chronology of Pliocene sea-level fluctuations: The U.S. Middle Atlantic Coastal Plain record , 1991 .
[30] N. Mahowald,et al. The PMIP 4 contribution to CMIP 6 – Part 4 : Scientific objectives and experimental design of the PMIP 4-CMIP 6 Last Glacial Maximum experiments and PMIP 4 sensitivity experiments , 2017 .
[31] Yan Zhao,et al. Evaluation of climate models using palaeoclimatic data , 2012 .
[32] S. McGregor,et al. The influence of non-stationary teleconnections on palaeoclimate reconstructions of ENSO variance using a pseudoproxy framework , 2015 .
[33] J. Lamarque,et al. AerChemMIP: quantifying the effects of chemistry and aerosols in CMIP6 , 2016 .
[34] David Pollard,et al. A data-constrained large ensemble analysis of Antarctic evolution since the Eemian , 2014 .
[35] Sandy P. Harrison,et al. DIRTMAP: the geological record of dust , 2001 .
[36] Steven J. Phipps,et al. Paleoclimate Data–Model Comparison and the Role of Climate Forcings over the Past 1500 Years* , 2013 .
[37] A. P. Siebesma,et al. The Cloud Feedback Model Intercomparison Project (CFMIP) , 2016 .
[38] M. Ziegler,et al. CO2 over the past 5 million years : Continuous simulation and new δ11B-based proxy data , 2016 .
[39] Andrew A. Kulpecz,et al. High tide of the warm Pliocene: Implications of global sea level for Antarctic deglaciation , 2012 .
[40] S. Rahmstorf,et al. Temperature-driven global sea-level variability in the Common Era , 2016, Proceedings of the National Academy of Sciences.
[41] D. Karoly,et al. Nonstationary Australasian Teleconnections and Implications for Paleoclimate Reconstructions , 2013 .
[42] Andrew A. Kulpecz,et al. deglaciation High tide of the warm Pliocene : Implications of global sea level for Antarctic , 2012 .
[43] Gregory J. L. Tourte,et al. The DeepMIP contribution to PMIP4: experimental design for model simulations of the EECO, PETM, and pre-PETM (version 1.0) , 2017 .
[44] A. Roberts,et al. Sea-level and deep-sea-temperature variability over the past 5.3 million years , 2014, Nature.
[45] Reto Knutti,et al. The Detection and Attribution Model Intercomparison Project (DAMIP v1.0)contribution to CMIP6 , 2016 .
[46] T. Zhou,et al. Effects of Large Volcanic Eruptions on Global Summer Climate and East Asian Monsoon Changes during the Last Millennium: Analysis of MPI-ESM Simulations , 2014 .
[47] Robert Pincus,et al. The Radiative Forcing Model Intercomparison Project (RFMIP): Experimental Protocol for CMIP6 , 2016 .
[48] K. Lambeck,et al. Sea level and global ice volumes from the Last Glacial Maximum to the Holocene , 2014, Proceedings of the National Academy of Sciences.
[49] P. Braconnot,et al. Tropical Pacific mean state and ENSO changes: sensitivity to freshwater flux and remnant ice sheets at 9.5 ka BP , 2015, Climate Dynamics.
[50] T. Zhou,et al. Simulation of the East Asian Summer Monsoon during the Last Millennium with the MPI Earth System Model , 2012 .
[51] T. L. Rasmussen,et al. Temporal and spatial structure of multi-millennial temperature changes at high latitudes during the Last Interglacial , 2014 .
[52] T. Stocker,et al. Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years , 2008, Nature.
[53] Corinne Le Quéré,et al. Role of Marine Biology in Glacial-Interglacial CO2 Cycles , 2005, Science.
[54] Caspar M. Ammann,et al. Climate forcing reconstructions for use in PMIP simulations of the last millennium (v1.0) , 2011 .
[55] E. Guilyardi,et al. ENSO at 6ka and 21ka from ocean–atmosphere coupled model simulations , 2008 .
[56] Pascale Braconnot,et al. Sensitivity of paleoclimate simulation results to season definitions , 1997 .
[57] Z. Liu,et al. Evolution and forcing mechanisms of El Niño over the past 21,000 years , 2014, Nature.
[58] T. Zhou,et al. Regional-scale surface air temperature and East Asian summer monsoon changes during the last millennium simulated by the FGOALS-gl climate system model , 2014, Advances in Atmospheric Sciences.
[59] D. Easterling,et al. Observations: Atmosphere and surface , 2013 .
[60] M. Kageyama,et al. Evaluation of CMIP5 palaeo-simulations to improve climate projections , 2015 .
[61] J. Fohlmeister,et al. Strong and deep Atlantic meridional overturning circulation during the last glacial cycle , 2014, Nature.
[62] J. Annan,et al. Can we trust climate models? , 2014 .
[63] P. Valdes,et al. How well do simulated last glacial maximum tropical temperatures constrain equilibrium climate sensitivity? , 2015 .
[64] Marie-Louise Siggaard-Andersen,et al. High-Resolution Greenland Ice Core Data Show Abrupt Climate Change Happens in Few Years , 2008, Science.
[65] I. Prentice,et al. Climate model benchmarking with glacial and mid-Holocene climates , 2014, Climate Dynamics.
[66] J. Fasullo,et al. Climate Variability and Change since 850 CE: An Ensemble Approach with the Community Earth System Model , 2016 .
[67] P. Braconnot,et al. Characterization of Model Spread in PMIP2 Mid-Holocene Simulations of the African Monsoon , 2013 .
[68] B. Otto‐Bliesner,et al. Critical evaluation of climate syntheses to benchmark CMIP6/PMIP4 127 ka Last Interglacial simulations in the high-latitude regions , 2017 .
[69] Eric Larour,et al. Ice Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6. , 2016, Geoscientific model development.
[70] A. Wittenberg. Are historical records sufficient to constrain ENSO simulations? , 2009 .
[71] André Berger,et al. Long-term variations of daily insolation and Quaternary climatic changes , 1978 .
[72] Michel Crucifix,et al. Does the Last Glacial Maximum constrain climate sensitivity? , 2006 .
[73] E. S. Epstein. On Obtaining Daily Climatological Values from Monthly Means , 1991 .
[74] Jacques Laskar,et al. A long-term numerical solution for the insolation quantities of the Earth , 2004 .
[75] Maureen E. Raymo,et al. Mid-Pliocene warmth: stronger greenhouse and stronger conveyor , 1996 .
[76] Chris Derksen,et al. LS3MIP (v1.0) Contribution to CMIP6: The Land Surface, Snow and Soil Moisture Model Intercomparison Project Aims, Setup and Expected Outcome. , 2016 .
[77] W. Lipscomb,et al. The PMIP4 contribution to CMIP6 – Part 2: Two interglacials, scientific objective and experimental design for Holocene and Last Interglacial simulations , 2016 .
[78] A. Moberg. A statistical hemispheric-scale climate model versus proxy data comparison , 2013 .
[79] G. Ramstein,et al. Mid-Pliocene East Asian monsoon climate simulated in the PlioMIP , 2013 .
[80] N. Graham,et al. Continental-scale temperature variability during the past two millennia , 2013 .
[81] S. Harrison,et al. Energy-balance mechanisms underlying consistent large-scale temperature responses in warm and cold climates , 2015, Climate Dynamics.
[82] François Massonnet,et al. The CMIP6 Sea-Ice Model Intercomparison Project (SIMIP): understanding sea ice through climate-model simulations , 2016 .
[83] P. Valdes,et al. Transient climate simulations of the deglaciation 21 – 9 thousand years before present ; PMIP 4 Core experiment design and boundary conditions , 2015 .
[84] B. Otto‐Bliesner,et al. A multi-model assessment of last interglacial temperatures , 2012 .
[85] L. Lisiecki,et al. A Late Pleistocene sea level stack , 2014 .
[86] T. Laepple,et al. Global and regional variability in marine surface temperatures , 2014 .
[87] M. Yoshimori,et al. Can the Last Glacial Maximum constrain climate sensitivity? , 2012 .
[88] M. Jansen,et al. Connecting Antarctic sea ice to deep-ocean circulation in modern and glacial climate simulations: SEA ICE AND GLACIAL AMOC , 2017 .
[89] Jung Choi,et al. Mid-Holocene tropical Pacific climate state, annual cycle, and ENSO in PMIP2 and PMIP3 , 2013, Climate Dynamics.
[90] E. Guilyardi,et al. Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints , 2006 .
[91] L. Bopp,et al. Modelling planktic foraminifer growth and distribution using an ecophysiological multi-species approach , 2011 .
[92] Thomas F. Stocker,et al. Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present , 2015 .
[93] D. Dilcher,et al. Oak leaves as biosensors of late Neogene and early Pleistocene paleoatmospheric CO2 concentrations , 1996 .
[94] L. Gallardo,et al. Dust fluxes and iron fertilization in Holocene and Last Glacial Maximum climates , 2015 .
[95] G. Marino,et al. Corrigendum: Sea-level and deep-sea-temperature variability over the past 5.3 million years , 2014, Nature.
[96] S. Harrison,et al. Precipitation scaling with temperature in warm and cold climates: An analysis of CMIP5 simulations , 2013 .
[97] R. Hatfield,et al. Evolution of the northeast Labrador Sea during the last interglaciation , 2012 .
[98] P. Valdes,et al. A new global biome reconstruction and data‐model comparison for the Middle Pliocene , 2008 .
[99] S. Rahmstorf,et al. Sea-level rise due to polar ice-sheet mass loss during past warm periods , 2015, Science.
[100] G. Faluvegi,et al. Global Signatures and Dynamical Origins of the Little Ice Age and Medieval Climate Anomaly , 2009, Science.
[101] Pierre Friedlingstein,et al. C4MIP – The Coupled Climate–Carbon Cycle Model Intercomparison Project: Experimental protocol for CMIP6 , 2016 .
[102] G. Leduc,et al. Implication of methodological uncertainties for Mid-Holocene sea surface temperature reconstructions , 2014 .
[103] N. Mahowald,et al. Twelve thousand years of dust: the Holocene global dust cycle constrained by natural archives , 2014 .
[104] J. Marotzke,et al. A model–data comparison for a multi-model ensemble of early Eocene atmosphere–ocean simulations: EoMIP , 2012 .
[105] P. Valdes,et al. Last glacial maximum radiative forcing from mineral dust aerosols in an Earth system model , 2015 .
[106] S. Harrison,et al. Consistent large‐scale temperature responses in warm and cold climates , 2013 .
[107] Joseph M. Prospero,et al. Global connections between aeolian dust, climate and ocean biogeochemistry at the present day and at the last glacial maximum , 2010 .
[108] D. Pollard,et al. A calendar conversion method for monthly mean paleoclimate model output with orbital forcing , 2002 .
[109] S. Bony,et al. Spread in model climate sensitivity traced to atmospheric convective mixing , 2014, Nature.
[110] M. Winstrup,et al. Timing and climate forcing of volcanic eruptions for the past 2,500 years , 2015, Nature.
[111] T. Quinn,et al. The record of Pliocene sea-level change at Enewetak Atoll , 1991 .
[112] Radford M. Neal,et al. A data-calibrated distribution of deglacial chronologies for the North American ice complex from glaciological modeling , 2012 .
[113] M. Yoshimori,et al. Dependency of Feedbacks on Forcing and Climate State in Physics Parameter Ensembles , 2011 .
[114] Zhonghui Liu,et al. High Earth-system climate sensitivity determined from Pliocene carbon dioxide concentrations , 2010 .
[115] G. Hegerl,et al. Small influence of solar variability on climate over the past millennium , 2014 .
[116] M. Raymo,et al. PLIOMAX: Pliocene maximum sea level project , 2009 .
[117] A. Tripati,et al. Coupling of CO2 and Ice Sheet Stability Over Major Climate Transitions of the Last 20 Million Years , 2009, Science.
[118] M. Kageyama,et al. Shortwave forcing and feedbacks in Last Glacial Maximum and Mid-Holocene PMIP3 simulations , 2015, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[119] S. Harrison,et al. Evaluation of modern and mid-Holocene seasonal precipitation of the Mediterranean and northern Africa in the CMIP5 simulations , 2014 .
[120] Veronika Eyring,et al. Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization , 2015 .
[121] Sandy P. Harrison,et al. Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP) , 1999 .
[122] M. Raymo,et al. A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ18O records , 2005 .
[123] J. Annan,et al. Skill and reliability of climate model ensembles at the Last Glacial Maximum and mid-Holocene , 2012 .
[124] B. Otto‐Bliesner,et al. Assessing confidence in Pliocene sea surface temperatures to evaluate predictive models , 2012 .
[125] E. Guilyardi,et al. Mid-Holocene and last glacial maximum climate simulations with the IPSL model: part II: model-data comparisons , 2013, Climate Dynamics.
[126] Angelyn W. Moore,et al. The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based on GPS positioning, exposure age dating of ice thicknesses, and relative sea level histories , 2014 .
[127] B. Otto‐Bliesner,et al. The Pliocene Model Intercomparison Project (PlioMIP) Phase 2: scientific objectives and experimental design , 2016 .
[128] D. Frierson,et al. Influence of West Antarctic Ice Sheet collapse on Antarctic surface climate , 2015 .